The source of "marine current" or "tidal stream" energy is the tide. When
we talk of marine current, we are referring to a moving mass of water with a velocity and direction.

Tides and tidal currents are generated by gravitational forces of the sun and moon on the
earth's waters. Due to its proximity to the earth, the moon exerts roughly twice the
tide raising force of the sun.

The gravitational forces of the sun and the moon create two "bulges" in the earth’s
oceans: one closest to the moon, and other on the opposite side of the globe. These
"bulges" result in the two tides (high water to low water sequence) a day -
the dominant tidal pattern in most of the world's oceans.

This is known as a semi-diurnal tide.

However, normally the tidal behaviour is not as simple the model on the right, instead behaving
similarly to the example below.

As the axis of the earth is tilted at 23.5 degrees to the moon’s orbit, the two bulges
are not equal unless the moon is over the equator.

This difference in
tide height between the two daily tides is called the diurnal (or declinational) inequality.
This repeats on a 14 day cycle as the moon rotates around the earth.

One cycle of high water to low water takes an average of 12.4 hours, although there
are occasional variations resulting in a lengthening or shortening of this time.

These variations have been analysed to understand the impact they might have on our
tidal model, so that any resultant error can be incorporated into
later calculations.

Spring tide is the very highest and very lowest tide (i.e. the largest tidal range) which occurs
twice a month (every 14/15 days) when the moon is either new or full (when the gravitational
pull of the sun and moon is aligned).
Neap tides are the opposite of the spring tide. The tidal range between high and low water is
smallest and occurs nearest the time of the first and last lunar quarters. The ratio of springs
to neaps can be as much as 2 to 1.

The combination of the spring to neaps cycle and the 14 day diurnal tidal cycle
results in a variability of the tides through the months of the year. There
are more than a hundred harmonic constituents (cyclic components) of the tide,
each with a different cycle time. These constituents combine so that tides only completely
repeat themselves every 18.6 years.

A 14 day analysis was implemented to assess the impact of this variation on power output from the
turbines.

Spring tide maximums vary throughout the year, as can be observed on the
graph above predicting
tidal heights for Dover 2004.

Many of the strongest tidal currents are located in shallow waters or through narrow channels that
connect large areas of water - hence the coastline and islands of the West of Scotland are an ideal
location for exploiting tidal currents.

The picture on the left shows the relationship between tidal
current (the dashed line) and tidal height (the solid line).

Halfway between high water and low
water is usually where the speed is at it's highest. The speed will be zero during the slack water
at high and low water (the peaks and troughs in the diagram).

In open water, the flow depends on the direction of the tidal wave.

In channels, the current is
constrained to flow either up or down the channel.

As you can see from the animation of tidal behaviour
in the Cook Straight in New Zealand on the left, the
currents change direction as we move from flood (tide in) to ebb (tide out).

The predicted tidal pattern can be modified by two factors, shown below:

Wind acting on the sea surface Vw - only has an impact to a certain depth below the surface.

Atmospheric pressure causing storm surges Vs.

Under exceptional conditions, these factors can raise tidal height by 2 or 3 metres or lower it
by 1 or 2 metres, having a subsequent impact on tidal current velocities.

Wind acting on the sea surface
may be an important consideration in exposed areas in winter months (depending upon turbine depth and
the corresponding barometric pressure).

The graph on the left for the 30 year average number of days with gales (1961 to 1990) at some typical
Scottish locations below shows how wind speeds can vary substaintially throughout the year.

Wherever possible, turbines will need to be located below the area of influence of the wind component of the current.

A third factor to consider is slack water. This is the period of quiet water when the tide
reverses from flood to ebb or vice versa. The duration of slack water will vary,
depending upon location and time of year. The tide change from flood (tide in) to ebb (tide out)
is referred to as high water slack. The tide change from ebb to flood is termed low water slack.

The "Rule of Twelfths" describes the varying power of the tide throughout its cycle.
Assuming a semi-diurnal tidal cycle and a period of approximately 6 hours between LW and HW,
then the rule states that in the:

1st hour after LW, 1 twelfth of the total water displaced travels.

2nd hour after LW, 2 twelfths of the total water displaced flows in.

3rd hour after, 3 twelfths of the total water displaced flows in.

4rd hour after, again 3 twelfths of the total water displaced flows in.

5th hour after, 2 twelfths of the total water travel in.

6th hour after, 1 twelfths comes in.

Therefore, the fastest streams take place during the 3rd and 4th hour after slack
water (HW or LW) when the largest amount of water travels (six twelfths or one half of the
total water displaced). The same pattern is true for the tide going out from HW to LW.

Despite the inherent predictability of tidal currents, we have identified a number of factors
which will vary the behaviour of the tidal currents from our standard model. Wherever possible,
errors have been calculated and stated alongside our results to ensure a robust analysis approach.